Use geometrized units and signature . The original PDF starts with the d'Alembert operator ; the local TeX incorrectly transcribes its derivative indices. The harmonic condition is the Lorenz gauge in linearized gravity.
Choose the retarded solution, excluding an incoming homogeneous wave. For a spatially localized source, the Linearized Einstein equations give
Let the source size be and the characteristic angular frequency be . Assume the weak-field approximation, nonrelativistic source velocities, and for a radiative far-zone measurement. Then . At leading order in and , one may replace the denominator by and the retarded time throughout the source by , obtaining
To identify this integral, use stress-energy conservation for a symmetric source tensor. Compact support or sufficient decay permits integration by parts with no boundary flux. Because in this signature, the second mass moment tensor satisfies
Spatial indices are raised with , so . Substitution gives the retarded quadrupole field:
The assumptions are an isolated conserved source, retarded boundary conditions, weak gravity, a source small compared with the wavelength, and observation far from it. The physical radiative field follows by the transverse-traceless projector applied to this trace-reversed metric perturbation.
The time-dependent components of the second mass moment tensor contain and . Taking two time derivatives for the retarded quadrupole field leaves that frequency unchanged. Hence the gravitational-wave frequency is
Here is angular frequency and counts cycles per unit time. If , the mass quadrupole moment is time independent, so the leading gravitational wave amplitude vanishes and there is no emitted quadrupole frequency to measure.